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Results:

• 31. VI_2015_005

  mean surface air temperature anomalies ....................................... 28 14 Surface air temperature anomalies over Scandinavia ...................................... 29 15 Composite mean precipitation anomalies..................................................... 30 6 1 Introduction Extratropical low-pressure systems, persisting for at least a few days, have long been recognised as one /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 32. Kok_JGEC658_2009

  to be simple and therefore has important drawbacks. Future improvements should be made in the light of applications within a larger toolbox of scenario methods.  2008 Elsevier Ltd. All rights reserved. * Tel.: +31 317 482422; fax: +31 317 419000. E-mail address: kasper.kok@wur.nl. Contents lists available at ScienceDirect Global Environmental Change journa l homepage: www.e lsev ier .com/ locate /media/loftslag/Kok_JGEC658_2009.pdf

• 33. Lorenzoni_Pidgeon_2006

  level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 34. VI_2022_006_extreme

  catchments in relation to CMIP5 climate scenarios . 27 5.2.1 Presentation of the climate datasets ................................................................... 27 5.2.2 Incorporation of the climate projections to the ICRA dataset ........................... 28 5.2.3 New 1M5 maps including climate projections .................................................. 31 5.2.4 New return levels /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 35. VI_2019_009

  - 26,83,84 - 27,87 - 70,71 - 72,73 - 74. ............................ 28 21 From left to right, the horizontal axis has the following SYNOP codes (manual station): The first is 10, the second is 11 & 41, the third is 40 and to the right is 46. 29 22 Number of records as a function of height of the 1st cloud layer from the manual and automatic stations /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 36. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 37. Refsgaard_etal-2007-Uncertainty-EMS

  and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 38. 2013_001_Nawri_et_al

  . . . . . . . . . . . . . . . . . 28 9 Weibull shape parameter at 50 and 100 mAGL for all wind directions . . . . . . . 30 10 Average wind power density based on corrected WRF model data . . . . . . . . . 33 11 Average wind power density based on NORA10 data . . . . . . . . . . . . . . . . 34 12 Differences in wind power density between northerly and southerly winds . . . . . 35 13 Directional /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 39. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 40. VI_Arsskyrsla_2018_vef

  grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf